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For many rocks, the sole A part of the P-T route recorded during the mineral assemblage and texture on the rock is the 'peak' of metamorphism -- the ailments of the thermal greatest (i.e., the maximum temperature as well as stress at the utmost temperature). If the rock had a sedimentary or volcanic protolith, you could infer that the rock started out within the surface, achieved peak conditions at some temperature and depth inside the Earth, and returned to your surface (exactly where the rock was gathered).

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compared to conditions of the peak of metamorphism symbolize disequilibrium. Generally, having said that, the evidence for disequilibrium can be extremely practical since it may be used to reconstruct P-T route segments.